Later Pleistocene/Holocene climate conditions of Qinghai–Xizhang Plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments-Reference-Cited by-同舟云学术

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Later Pleistocene/Holocene climate conditions of Qinghai–Xizhang Plateau (Tibet) based on carbon and oxygen stable isotopes of Zabuye Lake sediments

Published:2002-10 Issue:1 Volume:203 Page:461-477
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Wang R.L.,Scarpitta S.C.,Zhang S.C.,Zheng M.P.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference41 articles.

1. A 13,000-year climate record from western Tibet;Gasse;Nature,1991

2. Response of Lake Baikal ecosystem to climate forcing and pCO2 change over the last glacial/interglacial transition;Prokopenko;Earth Planet. Sci. Lett.,1999

3. An organic isotopic record of glacial–postglacial change in atmospheric pCO2 in the sediments of Lake Biwa, Japan;Meyers;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1993

4. Climatic and hydrological oscillations in the Ownes Lake Basin, and adjacent Sierra Nevada, California;Benson;Science,1996

5. Large-scale aspects of the summer monsoon in south and east Asia;Flohn;J. Meteorol. Soc. Jpn.,1957

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